Taxonomic and metabolic profiling of glacial ice algal communities on the Greenland Ice Sheet
Authors/Creators
- Lutz, Stefanie (Contact person)1, 2
- Majumder, Anirban (Researcher)1, 3
- Erban, Alexander (Researcher)4
- McCutcheon, Jenine (Researcher)5, 6
- Anesio, Alexandre M. (Researcher)7
- McQuaid, James B. (Researcher)5
- Tranter, Martyn (Researcher)7, 8
- Kopka, Joachim (Researcher)4
- Benning, Liane G. (Contact person)1, 3, 5
- 1. Interface Geochemistry, GFZ Helmholtz Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
- 2. Department of Plant and Microbial Biology, University of Zurich, Switzerland
- 3. Department of Earth Sciences, Freie Universität Berlin, 12249 Berlin, Germany
- 4. Max Planck Institute of Molecular Plant Physiology, Am Mühlenberg 1, 14476 Potsdam, Germany
- 5. School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK
- 6. Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, N2L 3G1, ON, Canada
- 7. Department of Environmental Science, Aarhus University, Roskilde, Denmark
- 8. School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, UK
Description
During the summer melt season, glacier ice algal blooms are widespread in the area termed “dark
zone” in the southwest region of Greenland. Due to their pigmentation, glacier ice algae reduce the
albedo of the ice sheet, increasing surface melting. Despite their crucial role in the Greenland Ice Sheet
(GrIS) ecosystem, we know little about their metabolic potential or functions. Here, we present insights
into the links between microbial community composition using 18S and ITS2 sequencing and total
metabolic profiling of samples dominated by glacier ice algae from the GrIS. Our analysis of ITS2
secondary structures reveals that blooms are dominated by a single algal species, yet glacier ice algal
haplotype composition differs between sites (along a 40 km transect) and surface habitats (clean snow
vs. high algal biomass ice). Furthermore, metabolic composition changes during the development of
glacier ice algal blooms with an accumulation of fatty acids, although few differences were observed
between sites along the transect. In addition, a few metabolites showed diurnal variations and our data
suggest that under low light and freezing conditions, chlorophyll degradation, tocopherol abundance
and phytol remobilization may be the key compounds changing in the glacier ice algae dominated
samples. Overall, these results improve our understanding of the chemical environment in the GrIS
supraglacial microbial community structure and the contribution of the primary producers dominated
by the glacier ice algae. Our data also show that endo- and exo-metabolic patterns need to be
differentiated and that multiplexed data sets will help gain a better insight into these complex algae-
controlled ecosystems.
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Metabolomics ice algae_ZONODO pre-print_27 Nov 2025.pdf
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